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Chamberlin–Moulton planetesimal hypothesis
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Chamberlin–Moulton planetesimal hypothesis
The
Chamberlin–Moulton planetesimal hypothesis
was proposed in 1905 by geologist
Thomas Chrowder Chamberlin
and astronomer
Forest Ray Moulton
to describe the formation of the
solar system
. It was proposed as a replacement for the
Laplacian
version of the
nebular hypothesis
that had prevailed since the 19th century.
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